TIME CONSTRAINTS ON THE FORMATION OF THE KANDALAKSHA AND KERETSK GRABENS OF THE WHITE SEA PALEO-RIFT SYSTEM FROM NEW ISOTOPIC GEOCHRONOLOGICAL DATA
Initially, the age and stratigraphic position of the Tersk formation were determined with respect to the fact that this formation overlaps the Early Proterozoic granitoids. Its top was marked by the rocks penetrated by the Late Devonian alkaline intrusions, including explosion pipes.This article pre...
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Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch
2021
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Online Access: | https://www.gt-crust.ru/jour/article/view/1241 https://doi.org/10.5800/GT-2021-12-3-0540 |
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Geodynamics & Tectonophysics (E-Journal) |
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Russian |
topic |
U–Pb датирование White Sea rift system (WSRS) Keretsk and Kandalaksha grabens Tersk formation detrital zircon grains U-Pb dating рифтовая система Белого моря Кандалакшский и Керецкий грабены терская свита зерна детритового циркона |
spellingShingle |
U–Pb датирование White Sea rift system (WSRS) Keretsk and Kandalaksha grabens Tersk formation detrital zircon grains U-Pb dating рифтовая система Белого моря Кандалакшский и Керецкий грабены терская свита зерна детритового циркона N. B. Kuznetsov A. S. Baluev E. N. Terekhov S. Yu. Kolodyazhnyi E. S. Przhiyalgovskii T. V. Romanyuk A. S. Dubensky V. S. Sheshukov S. M. Lyapunov T. B. Bayanova P. A. Serov Н. Б. Кузнецов А. С. Балуев Е. Н. Терехов С. Ю. Колодяжный Е. С. Пржиялговский Т. В. Романюк А. С. Дубенский В. С. Шешуков С. М. Ляпунов Т. Б. Баянова П. А. Серов TIME CONSTRAINTS ON THE FORMATION OF THE KANDALAKSHA AND KERETSK GRABENS OF THE WHITE SEA PALEO-RIFT SYSTEM FROM NEW ISOTOPIC GEOCHRONOLOGICAL DATA |
topic_facet |
U–Pb датирование White Sea rift system (WSRS) Keretsk and Kandalaksha grabens Tersk formation detrital zircon grains U-Pb dating рифтовая система Белого моря Кандалакшский и Керецкий грабены терская свита зерна детритового циркона |
description |
Initially, the age and stratigraphic position of the Tersk formation were determined with respect to the fact that this formation overlaps the Early Proterozoic granitoids. Its top was marked by the rocks penetrated by the Late Devonian alkaline intrusions, including explosion pipes.This article presents the U-Pb isotopic dating of detrital zircon grains (dZr) from sandstones of the Tersk formation. It describes the geochemical compositions of the rocks and the Sm-Nd study results. In our study, the weighted average age of four youngest dZr grains from the sandstones of the Tersk formation is 1145±20 Ma, which suggests that the rocks above the studied rock layer (see the Tersk formation cross-section) are is not older than the end of the Middle Riphean. The U-Pb isotopic ages of dZr grains (provenance signals) from the sandstones of the Tersk formation were compared to the ages of other Upper Precambrian clastic strata in the northeastern East European platform (EEP) and adjacent areas. Our comparative analysis shows that these rocks significantly differ in age. This conclusion is in good agreement with the idea that at the end of the Middle and during the Late Riphean, several small (mainly closed) basins separated by uplifts dominated in the paleogeographic setting of the area wherein the White Sea rift system (WSRS) formed and developed. Temporal connections of these basins with the ocean were possible. Such paleogeographic setting does not favour the development of large rivers; this is why the grabens are mainly filled with local rock materials. The Keretsk and Kandalaksha grabens (WSRS) are filled with marine sediments eroded from the grabens walls. The local sediment sources include eclogite complexes (~1.9 Ga), which basic magmatism is dated at ~2.4–2.5 and ~2.7–2.9 Ga. Any potential primary sources for dZr grains are lacking in the area near the Keretsk graben. We suggest that such grains occurred due to recycling of the secondary sources of zircon, i.e. originated from ancient local sedimentary ... |
author2 |
The study was budgeted by the Geological Institute RAS (Laboratory budget) and supported by the Russian Foundation for Basic Research (Project 18-05-00485). The geochronological data were consolidated and systematized with the financial support of the RF Ministry of Education and Science (Megagrant 075-15-2019-1883 – Orogenesis: Formation and Growth of Continents and Supercontinents). Работа выполнена в рамках бюджетной темы лаборатории ГИН РАН при поддержке РФФИ, проект № 18-05-00485. Сбор и систематизация геохронологических данных выполнены при финансовой поддержке МОН РФ (мегагрант 075-15-2019-1883, «Орогенез: образование и рост континентов и суперконтинентов»). |
format |
Article in Journal/Newspaper |
author |
N. B. Kuznetsov A. S. Baluev E. N. Terekhov S. Yu. Kolodyazhnyi E. S. Przhiyalgovskii T. V. Romanyuk A. S. Dubensky V. S. Sheshukov S. M. Lyapunov T. B. Bayanova P. A. Serov Н. Б. Кузнецов А. С. Балуев Е. Н. Терехов С. Ю. Колодяжный Е. С. Пржиялговский Т. В. Романюк А. С. Дубенский В. С. Шешуков С. М. Ляпунов Т. Б. Баянова П. А. Серов |
author_facet |
N. B. Kuznetsov A. S. Baluev E. N. Terekhov S. Yu. Kolodyazhnyi E. S. Przhiyalgovskii T. V. Romanyuk A. S. Dubensky V. S. Sheshukov S. M. Lyapunov T. B. Bayanova P. A. Serov Н. Б. Кузнецов А. С. Балуев Е. Н. Терехов С. Ю. Колодяжный Е. С. Пржиялговский Т. В. Романюк А. С. Дубенский В. С. Шешуков С. М. Ляпунов Т. Б. Баянова П. А. Серов |
author_sort |
N. B. Kuznetsov |
title |
TIME CONSTRAINTS ON THE FORMATION OF THE KANDALAKSHA AND KERETSK GRABENS OF THE WHITE SEA PALEO-RIFT SYSTEM FROM NEW ISOTOPIC GEOCHRONOLOGICAL DATA |
title_short |
TIME CONSTRAINTS ON THE FORMATION OF THE KANDALAKSHA AND KERETSK GRABENS OF THE WHITE SEA PALEO-RIFT SYSTEM FROM NEW ISOTOPIC GEOCHRONOLOGICAL DATA |
title_full |
TIME CONSTRAINTS ON THE FORMATION OF THE KANDALAKSHA AND KERETSK GRABENS OF THE WHITE SEA PALEO-RIFT SYSTEM FROM NEW ISOTOPIC GEOCHRONOLOGICAL DATA |
title_fullStr |
TIME CONSTRAINTS ON THE FORMATION OF THE KANDALAKSHA AND KERETSK GRABENS OF THE WHITE SEA PALEO-RIFT SYSTEM FROM NEW ISOTOPIC GEOCHRONOLOGICAL DATA |
title_full_unstemmed |
TIME CONSTRAINTS ON THE FORMATION OF THE KANDALAKSHA AND KERETSK GRABENS OF THE WHITE SEA PALEO-RIFT SYSTEM FROM NEW ISOTOPIC GEOCHRONOLOGICAL DATA |
title_sort |
time constraints on the formation of the kandalaksha and keretsk grabens of the white sea paleo-rift system from new isotopic geochronological data |
publisher |
Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch |
publishDate |
2021 |
url |
https://www.gt-crust.ru/jour/article/view/1241 https://doi.org/10.5800/GT-2021-12-3-0540 |
long_lat |
ENVELOPE(32.417,32.417,67.133,67.133) |
geographic |
White Sea Kandalaksha |
geographic_facet |
White Sea Kandalaksha |
genre |
Arctic White Sea Белого моря |
genre_facet |
Arctic White Sea Белого моря |
op_source |
Geodynamics & Tectonophysics; Том 12, № 3 (2021); 570-607 Геодинамика и тектонофизика; Том 12, № 3 (2021); 570-607 2078-502X |
op_relation |
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ftjgat:oai:oai.gtcrust.elpub.ru:article/1241 2023-05-15T14:28:32+02:00 TIME CONSTRAINTS ON THE FORMATION OF THE KANDALAKSHA AND KERETSK GRABENS OF THE WHITE SEA PALEO-RIFT SYSTEM FROM NEW ISOTOPIC GEOCHRONOLOGICAL DATA О ВРЕМЕНИ ФОРМИРОВАНИЯ КАНДАЛАКШСКОГО И КЕРЕЦКОГО ГРАБЕНОВ ПАЛЕОРИФТОВОЙ СИСТЕМЫ БЕЛОГО МОРЯ В СВЕТЕ НОВЫХ ДАННЫХ ИЗОТОПНОЙ ГЕОХРОНОЛОГИИ N. B. Kuznetsov A. S. Baluev E. N. Terekhov S. Yu. Kolodyazhnyi E. S. Przhiyalgovskii T. V. Romanyuk A. S. Dubensky V. S. Sheshukov S. M. Lyapunov T. B. Bayanova P. A. Serov Н. Б. Кузнецов А. С. Балуев Е. Н. Терехов С. Ю. Колодяжный Е. С. Пржиялговский Т. В. Романюк А. С. Дубенский В. С. Шешуков С. М. Ляпунов Т. Б. Баянова П. А. Серов The study was budgeted by the Geological Institute RAS (Laboratory budget) and supported by the Russian Foundation for Basic Research (Project 18-05-00485). The geochronological data were consolidated and systematized with the financial support of the RF Ministry of Education and Science (Megagrant 075-15-2019-1883 – Orogenesis: Formation and Growth of Continents and Supercontinents). Работа выполнена в рамках бюджетной темы лаборатории ГИН РАН при поддержке РФФИ, проект № 18-05-00485. Сбор и систематизация геохронологических данных выполнены при финансовой поддержке МОН РФ (мегагрант 075-15-2019-1883, «Орогенез: образование и рост континентов и суперконтинентов»). 2021-09-17 application/pdf https://www.gt-crust.ru/jour/article/view/1241 https://doi.org/10.5800/GT-2021-12-3-0540 rus rus Institute of the Earth's crust of the Russian Academy of Sciences, Siberian Branch https://www.gt-crust.ru/jour/article/view/1241/568 Andreichev V.L., Soboleva A.A., Gehrels G., 2014. U-Pb Dating and Provenance of Detrital Zircons from the Upper Precambrian Deposits of North Timan. 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CC-BY Geodynamics & Tectonophysics; Том 12, № 3 (2021); 570-607 Геодинамика и тектонофизика; Том 12, № 3 (2021); 570-607 2078-502X U–Pb датирование White Sea rift system (WSRS) Keretsk and Kandalaksha grabens Tersk formation detrital zircon grains U-Pb dating рифтовая система Белого моря Кандалакшский и Керецкий грабены терская свита зерна детритового циркона info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2021 ftjgat https://doi.org/10.5800/GT-2021-12-3-0540 https://doi.org/10.1134/s0869593814020026 https://doi.org/10.1134/S0016852106030034 https://doi.org/10.31857/S0016-853X2019162-86 https://doi.org/10.1134/S1028334X12060207 https://doi.org/10.1144/GSL.SP. 2022-07-19T15:36:33Z Initially, the age and stratigraphic position of the Tersk formation were determined with respect to the fact that this formation overlaps the Early Proterozoic granitoids. Its top was marked by the rocks penetrated by the Late Devonian alkaline intrusions, including explosion pipes.This article presents the U-Pb isotopic dating of detrital zircon grains (dZr) from sandstones of the Tersk formation. It describes the geochemical compositions of the rocks and the Sm-Nd study results. In our study, the weighted average age of four youngest dZr grains from the sandstones of the Tersk formation is 1145±20 Ma, which suggests that the rocks above the studied rock layer (see the Tersk formation cross-section) are is not older than the end of the Middle Riphean. The U-Pb isotopic ages of dZr grains (provenance signals) from the sandstones of the Tersk formation were compared to the ages of other Upper Precambrian clastic strata in the northeastern East European platform (EEP) and adjacent areas. Our comparative analysis shows that these rocks significantly differ in age. This conclusion is in good agreement with the idea that at the end of the Middle and during the Late Riphean, several small (mainly closed) basins separated by uplifts dominated in the paleogeographic setting of the area wherein the White Sea rift system (WSRS) formed and developed. Temporal connections of these basins with the ocean were possible. Such paleogeographic setting does not favour the development of large rivers; this is why the grabens are mainly filled with local rock materials. The Keretsk and Kandalaksha grabens (WSRS) are filled with marine sediments eroded from the grabens walls. The local sediment sources include eclogite complexes (~1.9 Ga), which basic magmatism is dated at ~2.4–2.5 and ~2.7–2.9 Ga. Any potential primary sources for dZr grains are lacking in the area near the Keretsk graben. We suggest that such grains occurred due to recycling of the secondary sources of zircon, i.e. originated from ancient local sedimentary ... Article in Journal/Newspaper Arctic White Sea Белого моря Geodynamics & Tectonophysics (E-Journal) White Sea Kandalaksha ENVELOPE(32.417,32.417,67.133,67.133) Geodynamics & Tectonophysics 12 3 570 607 |